The Characteristics and Seepage Stability Analysis of Toppling-Sliding Failure under Rainfall

Toppling-sliding failure is a typical mode of deep-seated toppling failure. In this mode, massive collapsed rock masses form the main sliding body, which is sensitive to rainfall events and prone to instability under rainfall due to its unique slope structure. In the present study, based on the detailed investigation on the geology and deformation characteristics, we studied the deformation and failure mechanism of a large-scale deep-seated toppling in Nandongzi Village, Pingquan City, Hebei Province. We constructed an engineering geology model to describe the toppling-sliding failure under rainfall. In addition, based on the saturated–unsaturated seepage theory and using the SLOPE/W and SEEP/W modules in the GeoStudio software, we explored the seepage law and factors controlling the seepage failure of toppling-sliding under rainfall. From surface to interior, the slope can be divided into topplingalling zone, strong toppling zone, slight toppling zone, and non-deformation zone. The geological structure consisting of an upper strong slab and an underlying weak rock layer, controls the early deformation, and the deformation and failure mode is compressing-bending-toppling. Due to the influence of excavation and rainfall, the sliding movements occur along planar rupture planes in the toppling-falling zone in the later stage, during which the failure mode switches to creeping-cracking. At present, the stability of the slope is highly sensitive to rainfall. When the rainfall intensity exceeds 220 mm/day (50 years return period storm), the factor of safety will fall below 1.05 and subsequently the sliding failure may be triggered. Because of the difference in permeability characteristics between the toppling-falling zone and the strong toppling zone, high pore-water pressure is developed at their boundary, leading to a drastic decrease in the factor of safety. Specifically, the more considerable difference in permeability, the lower the safety factor. Overall, this study is significant in scientific guiding for evaluating and preventing such slope failures.

[1]  Yifei Gong,et al.  Deformation and Failure Mechanism of a Massive Ancient Anti-Dip River-Damming Landslide in the Upper Jinsha River , 2022, Sustainability.

[2]  Jian-ye Huang,et al.  Stability Analysis of a High-Steep Dump Slope under Different Rainfall Conditions , 2022, Sustainability.

[3]  Da Huang,et al.  Deep-seated toppling deformations of rock slopes in western China , 2022, Landslides.

[4]  Huiming Tang,et al.  A complex rockslide developed from a deep-seated toppling failure in the upper Lancang River, Southwest China , 2021 .

[5]  Tolga Görüm,et al.  Spatiotemporal variations of fatal landslides in Turkey , 2021, Landslides.

[6]  Vantuan Nguyen,et al.  The critical curve for shallow saturated zone in soil slope under rainfall and its prediction for landslide characteristics , 2021, Bulletin of Engineering Geology and the Environment.

[7]  Xuanmei Fan,et al.  Prediction of shallow landslides in pyroclastic-covered slopes by coupled modeling of unsaturated and saturated groundwater flow , 2020, Landslides.

[8]  Sung-Eun Cho,et al.  Slope Stability Analysis of Unsaturated Soil Slopes Based on the Site-Specific Characteristics: A Case Study of Hwangryeong Mountain, Busan, Korea , 2020, Sustainability.

[9]  S. Loew,et al.  From Toppling to Sliding: Progressive Evolution of the Moosfluh Landslide, Switzerland , 2019, Journal of Geophysical Research: Earth Surface.

[10]  Bill X. Hu,et al.  Characterizing groundwater flow in a translational rock landslide of southwestern China , 2019, Bulletin of Engineering Geology and the Environment.

[11]  S. Evans,et al.  Mechanics of the earthquake-induced Hongshiyan landslide in the 2014 Mw 6.2 Ludian earthquake, Yunnan, China , 2019, Engineering Geology.

[12]  R. Greco,et al.  Interaction between Perched Epikarst Aquifer and Unsaturated Soil Cover in the Initiation of Shallow Landslides in Pyroclastic Soils , 2018, Water.

[13]  Giovanni B. Crosta,et al.  Deep seated gravitational slope deformations in the European Alps , 2013 .

[14]  Yong Li,et al.  Mass wasting triggered by the 2008 Wenchuan earthquake is greater than orogenic growth , 2011 .

[15]  L. Alejano,et al.  Analysis of a complex toppling-circular slope failure , 2010 .

[16]  Harianto Rahardjo,et al.  A simple model for preliminary evaluation of rainfall-induced slope instability , 2009 .

[17]  M. Anderson,et al.  Landslide Hazard and Risk: Glade/Landslide , 2005 .

[18]  Delwyn G. Fredlund,et al.  Numerical study of soil conditions under which matric suction can be maintained , 2004 .

[19]  Oldrich Hungr,et al.  Large-scale brittle and ductile toppling of rock slopes , 2002 .

[20]  Charles Wang Wai Ng,et al.  A numerical investigation of the stability of unsaturated soil slopes subjected to transient seepage , 1998 .

[21]  D. Fredlund,et al.  Soil Mechanics for Unsaturated Soils: Fredlund/Soil Mechanics for Unsaturated Soils , 1993 .

[22]  Van Genuchten,et al.  A closed-form equation for predicting the hydraulic conductivity of unsaturated soils , 1980 .

[23]  D. Fredlund,et al.  The shear strength of unsaturated soils , 1978 .

[24]  E. L. Matyas,et al.  Volume Change Characteristics of Partially Saturated Soils , 1968 .

[25]  K. Sassa,et al.  Landslide Science for a Safer Geoenvironment: Volume 2: Methods of Landslide Studies , 2014 .

[26]  Y. Onda,et al.  Characterization of the groundwater response to rainfall on a hillslope with fractured bedrock by creep deformation and its implication for the generation of deep-seated landslides on Mt. Wanitsuka, Kyushu Island , 2014 .

[27]  Sun Huaikun Analysis of seepage stability of large-scale landslide under rainfall condition , 2013 .

[28]  G Crosta,et al.  Landslide, spreading, deep seated gravitational deformation: analysis, examples, problems and proposals , 1997 .